SIAM J. APPLIED DYNAMICAL SYSTEMS c 2004 Society for Industrial and Applied Mathematics Vol. 3, No. 3, pp. 352–377
Tippe Top Inversion as a Dissipation-Induced Instability∗
† ‡ § Nawaf M. Bou-Rabee , Jerrold E. Marsden , and Louis A. Romero
Abstract. By treating tippe top inversion as a dissipation-induced instability, we explain tippe top inversion through a system we call the modified Maxwell–Bloch equations. We revisit previous work done on this problem and follow Or’s mathematical model [SIAM J. Appl. Math., 54 (1994), pp. 597–609]. A linear analysis of the equations of motion reveals that only the equilibrium points correspond to the inverted and noninverted states of the tippe top and that the modified Maxwell–Bloch equations describe the linear/spectral stability of these equilibria. We supply explicit criteria for the spectral stability of these states. A nonlinear global analysis based on energetics yields explicit criteria for the existence of a heteroclinic connection between the noninverted and inverted states of the tippe top. This criteria for the existence of a heteroclinic connection turns out to agree with the criteria for spectral stability of the inverted and noninverted states. Throughout the work we support the analysis with numerical evidence and include simulations to illustrate the nonlinear dynamics of the tippe top.
Key words. tippe top inversion, dissipation-induced instability, constrained rotational motion, axisymmetric rigid body
AMS subject classifications. 70E18, 34D23, 37J15, 37M05
DOI. 10.1137/030601351
1. Introduction. Tippe tops come in a variety of forms. The most common geometric form is a cylindrical stem attached to a truncated ball, as shown in Figure 1.1. On a flat surface, the tippe top will rest stably with its stem up. However, spun fast enough on its blunt end, the tippe top momentarily defies gravity, inverts, and spins on its stem until dissipation causes it to fall over. This spectacular sequence of events occurs because, and in spite of, dissipation. Tippe top inversion is an excellent example of a dissipation-induced instability. Tippe top inversion is described by a system we call the modified Maxwell–Bloch equations. These
∗Received by the editors October 22, 2003; accepted for publication (in revised form) by M. Golubitsky January 22, 2004; published electronically July 6, 2004. This work was performed by an employee of the U.S. Government or under U.S. Government contract. The U.S. Government retains a nonexclusive, royalty-free license to publish or reproduce the published form of this contribution, or allow others to do so, for U.S. Government purposes. Copyright is owned by SIAM to the extent not limited by these rights. http://www.siam.org/journals/siads/3-3/60135.html †Applied and Computational Mathematics, Caltech, Pasadena, CA 91125 ([email protected]). The research of this author was supported by the U.S. DOE Computational Science Graduate Fellowship through grant DE-FG02- 97ER25308. ‡Control and Dynamical Systems, Caltech, Pasadena, CA 91125 ([email protected]). The research of this author was partially supported by the National Science Foundation. §Sandia National Laboratories, P.O. Box 5800, MS 1110, Albuquerque, NM 87185-1110 ([email protected]). The research of this author was supported by Sandia National Laboratories. Sandia is a multiprogram laboratory operated by Sandia Corporation, a Lockheed Martin Company, for the United States Department of Energy under contract DE-AC04-94AL85000. 352 TIPPE TOP INVERSION 353
Figure 1.1. From left: a sketch of the noninverted and inverted states of the tippe top. equations are a generalization of a previously derived normal form describing dissipation- induced instabilities in the neighborhood of the 1:1 resonance [4]. We will show in section 2 that the modified Maxwell–Bloch equations are the normal form for rotationally symmetric, planar dynamical systems. A dissipation-induced instability describes a neutrally stable equilibrium becoming spec- trally (and hence nonlinearly) unstable with the addition of dissipation. Dissipation-induced instability itself has a long history, which goes back to Thomson and Tait; see [14]. In its modern form, dissipation-induced instability was shown both to be a general phenomenon for gyroscopically stabilized systems and to provide a sharp converse to the energy momen- tum stability method by Bloch et al. in [1] and [2]. We refer the reader to these papers for additional examples and basic theory. By considering tippe top inversion as a dissipation-induced instability, we observe pre- cisely how tippe top inversion relates to well-understood dissipation-induced instabilities in gyroscopic systems.
History and literature. Tippe top inversion has been much investigated in the literature but never satisfactorily resolved. In what follows we survey a selection of theoretical results relevant to this paper. We refer the reader to the work of Cohen [5] and Or [11] for more comprehensive surveys of the literature. Analysis of the tippe top dates back to the last century with Routh’s commentary on the rising of tops. Routh’s simple physical analysis made it clear that dissipation was fundamental in understanding the physics of tippe top inversion [12]. In 1977, Cohen confirmed Routh’s physical analysis through numerical simulation [5]. Cohen modeled the tippe top as a holo- nomic ball with an inhomogeneous, axisymmetric mass distribution on a fixed plane. Thus, the ball’s center of mass was on its axis of symmetry, but not coincident with its geometric center. Tippe top inversion corresponded to the ball’s center of gravity moving above its ge- ometric center. Cohen’s mathematical model, derived using Newtonian mechanics, is written in terms of Euler angles and assumed a sliding friction law. In reality, tippe top inversion is a transient phenomenon because of dissipation. How- ever, by neglecting frictional torque, the spinning inverted state becomes a steady-state phe- nomenon. With a sliding friction law that neglects frictional torque, Cohen’s equations of motion were amenable to a linear-stability analysis about the spinning inverted and nonin- verted states, but he did not carry out such an analysis in his work. In this sense the fact that the model neglects frictional torque is a feature rather than a defect of the friction law. Cohen concluded that a sliding friction law based on Coulomb friction explains tippe top 354 NAWAF M. BOU-RABEE, JERROLD E. MARSDEN, AND LOUIS A. ROMERO inversion. Moreover, Cohen showed that the inviscid ball (no sliding friction) does not invert. Coulomb friction is proportional to the normal force exerted by the surface at the point of contact and opposes the motion of the tippe top at the point of contact. This nonlinear friction law drops out of a standard linear-stability analysis. In 1994, Or extended Cohen’s work by generalizing his friction law, performing a dimen- sional analysis of the equations of motion, writing the equations of motion in convenient coordinates, and exploring the linearized behavior of the ball. To further facilitate a linear- stability analysis, Or added viscous friction to Cohen’s friction law. The viscous friction is linearly related to the slip velocity at the point of contact. Or’s work showed that inversion could occur because of viscous or Coulomb friction. Or’s analysis of tippe top inversion by Coulomb friction and viscous friction demonstrated viscous friction flips the top more rapidly than Coulomb friction. His analysis mentioned first integrals in the no-slip problem, but did not use them to explain the global behavior of the tippe top. There was good reason to avoid a global analysis of the tippe top: the theoretical model of a ball did not accurately model the contact effects of the tippe top stem. However, the fundamental physics behind the global behavior of the tippe top was still reasonably described by the equations of motion for a ball with an eccentric center of mass, i.e., a gyroscopic, axisymmetric rigid body rising from a gravitationally favorable position to an unfavorable one because of dissipation. This observation motivated some aspects of the present study and possibly Ebenfeld’s thesis on tippe top inversion from a Lyapunov perspective. In 1995, Ebenfeld and Scheck applied a Lyapunov method to a dimensional version of Or’s mathematical model. Using the energy as a Lyapunov function, they analyzed the orbital sta- bility of the spinning, sliding ball. They showed that, starting with nonzero slip, the standing, spinning tippe top tends to manifolds of constant energy with no-slip and no tangential surface force. Moreover, they showed that without slip the tippe top cannot invert. They classified all possible asymptotic solutions as either tumbling (precession, spin, and no nutation) or rotating (pure spin) solutions. They provide criteria for determining the Lyapunov stability of these solutions [6]. We have applied some techniques of the present work to the related, but different, “rising egg” problem. (See Bou-Rabee, Marsden, and Romero [3].) In that paper we address the contributions of Moffatt [10] and Ruina [13] to that problem.
Main goals of this paper. The main result of this paper asserts that the stability of the noninverted and inverted tippe top (cf. Figure 1.1) and the existence of a heteroclinic connec- tion between these states is completely described by the modified Maxwell–Bloch equations: a normal form for rotationally symmetric, planar dynamical systems. This result is important because (1) it shows how tippe top inversion relates to well-studied dissipation-induced insta- bilities in gyroscopic systems; (2) it integrates the linear and nonlinear analysis; and (3) it simplifies the analysis of tippe top inversion and yields explicit criteria for when the tippe top inverts. We use Or’s mathematical model with viscous friction to obtain equations of motion for the tippe top in a convenient set of coordinates. We locate and analyze the stability of all equilibrium points of the equations of motion. As Ebenfeld observed, the viscous problem conserves ΥQ, the angular momentum about the vector connecting the center of mass of the TIPPE TOP INVERSION 355 ball to the surface point of contact. For a fixed value of ΥQ, the only equilibrium points of the equations of motion correspond to the noninverted and inverted states of the tippe top. We extend Or’s linear analysis by linearizing about both of these equilibrium points. By assuming that the translation of the center of mass is negligible, we derive a reduced system for the tippe top in terms of only angular variables. We show that this reduced equation is of the form of a modified Maxwell–Bloch equation and give reasons to support this approx- imation. Analysis of explicit stability criteria for the reduced system shows that the reduced system accurately describes the linearized behavior of the tippe top. Thus, the paper shows that the stability of the noninverted and inverted tippe top is completely determined by the modified Maxwell–Bloch equations. Moreover, these equations are the normal form for tippe top inversion; i.e., they are the simplest possible equations that can capture tippe top inversion. We extend the nonlinear analysis by proving the existence of a heteroclinic connection be- tween the noninverted and inverted states of the tippe top. Application of LaSalle’s invariance principle repeats/simplifies Ebenfeld’s energy arguments. Like Ebenfeld, we use the energy as a Lyapunov function. For the viscous problem, we show that the energy’s orbital derivative is negative semidefinite and a constant multiple of the 2-norm of the slip velocity. Thus, when the slip velocity vanishes, the energy is conserved. We identify the largest invariant set on this manifold characterized by no-slip and no tangential surface force. The largest invariant set on this manifold extremizes the energy subject to the surface and angular momentum constraint: ΥQ = constant. For certain parameter values, we find that the noninverted and inverted equilibrium states are the only extrema of the energy and are, in fact, the absolute maxima and minima of the energy, respectively. By the theorems of Barbashin and Krasovskii, trajectories starting in the neighborhood of the asymptotically unstable, noninverted state approach the asymptotically stable, inverted state as t →∞; i.e., the inverted state is globally asymptotically stable [8]. Outside this range of parameter values, the inverted and noninverted states become asymptotically unstable and a limit cycle corresponding to Ebenfeld’s tumbling solution minimizes the energy. Thus, the asymptotic states of the tippe top approach either (i) an isolated asymptotically stable equilibrium point or (ii) a neutrally stable limit cycle. The second case corresponds to the inverted and noninverted states being asymptotically unstable. In this case trajectories starting in the neighborhood of the noninverted, asymptotically unstable state will tend to limit cycles upon which total energy, magnitude of the angular momentum, nutation angle, and angular momentum about the vertical are conserved. We refer the reader to Ebenfeld for conditions for Lyapunov stability of this limit cycle. When the inverted state is asymptotically stable, a heteroclinic connection between the asymptotically unstable and stable states of the tippe top exists. We derive explicit criteria to determine the range of parameter values for which the heteroclinic connection exists. A comparison of the existence criteria for the heteroclinic connection and the linear- stability criteria derived from the modified Maxwell–Bloch system for the tippe top shows they are explicitly related. Thus, the modified Maxwell–Bloch equations fully explain tippe top inversion. Without dissipation, linear theory concludes that the equilibria are linearly (or neutrally) stable, which does not imply nonlinear stability. With dissipation, however, it is no surprise that the linear analysis provides the correct local nonlinear dynamics (since dissipation moves 356 NAWAF M. BOU-RABEE, JERROLD E. MARSDEN, AND LOUIS A. ROMERO eigenvalues off of the imaginary axis). Organization of the paper. In section 2, we present the modified Maxwell–Bloch equa- tions. We derive these equations and supply specific stability criteria for the system’s char- acteristic polynomial. We also discuss the ability of this model to capture the fundamental physics in tippe top inversion. In section 3, we derive and discuss the mathematical model of the tippe top. Specifically, we write the dimensional equations of motion of the theoretical tippe top using Newtonian mechanics, discuss the friction law, and nondimensionalize these equations. We also explicitly compare the model in this paper to others in the literature. In section 4, we apply linear theory to the nonlinear model. In particular, we locate the equilibria of the governing dimensionless equations, linearize about these states, as well as review and extend Or’s numerical stability analysis. In section 5, we cast the linearized equations for the tippe top in the form of the modified Maxwell–Bloch equations. We mention a direct derivation to these equations and analyze the stability of the modified Maxwell–Bloch equations. In particular, we show that these equations are the simplest possible equations that can capture the fundamental physics in tippe top inversion. In section 6, we explain tippe top inversion from an energy landscape perspective. We apply LaSalle’s invariance principle to determine the asymptotic state of the tippe top, study the behavior of solutions on this asymptotic state, and determine when this asymptotic state corresponds to the inverted tippe top. We also compare the criteria for the existence of a heteroclinic connection with the linear-stability criteria for the tippe top modified Maxwell– Bloch equations provided in section 5. In section 7, we discuss data from simulations which verify the local and global analysis in the paper. We conclude the paper with a discussion of future directions inspired by this work. 2. Modified Maxwell–Bloch equations. This section introduces an important extension of the Maxwell–Bloch equations and studies their stability. Derivation. Consider a planar ODE of the form x q¨ = f(q, q˙),q= . y
Linearization of these equations yields
q¨ = Aq˙ + Bq.
The characteristic polynomial of this system σ2 0 det + Aσ + B =0 0 σ2 shows that the ODE will have time-reversal symmetry; i.e., if σ is a solution, then so is −σ, when A is skew-symmetric and B is symmetric. TIPPE TOP INVERSION 357
We define the rotation matrix cos(θ) − sin(θ) R(θ)= sin(θ) cos(θ) as well as the identity and elementary skew-symmetric matrix in R2: 10 0 −1 I = ,S= . 01 10
The necessary and sufficient condition for a 2 × 2 matrix in R2 to commute with the rotation matrix is that the matrix be a linear combination of I and S. Thus, if this ODE is rotationally symmetric, i.e., the ODE is invariant under SO(2) rota- tion, then the matrices A and B can be expressed as
A = −αS − βI, B = −γS − δI, where α, β, γ, and δ are real scalars. Because α and γ can destroy time-reversal symmetry in A and B, we call these terms dissipative. Given the particular form of the rotationally symmetric ODE, we can write the two- dimensional real system as a one-dimensional complex system,
(2.1) z¨ + iαz˙ + βz˙ + iγz + δz =0,z= x + iy, which we call the modified Maxwell–Bloch equations. We observe that (2.1) is the basic harmonic oscillator with the two complex terms iαz˙ and iγz. In physical systems, the first term arises from Coriolis effects, and hence is known as the gyroscopic term. The second term typically arises from dissipation in rotational variables. This damping force is different from the usual damping term proportional to absolute velocity, βz˙. Physically the complex damping term models viscous effects caused by, for example, motion in a fluid, while the usual damping term models internal dissipation. Proposition 2.1. The modified Maxwell–Bloch equations are the linearized normal form for planar, rotationally symmetric dynamical systems. Stability criteria. The characteristic polynomial of the modified Maxwell–Bloch equations is
λ4 +2βλ3 +(α2 + β2 +2δ)λ2 +2(αγ + βδ)λ +(γ2 + δ2)=0.
We now write the necessary and sufficient conditions for this polynomial to be Hurwitz [7]. Proposition 2.2. The zero solution of the modified Maxwell–Bloch equations is asymptoti- cally stable provided that the following inequalities hold:
β>0, (2.2) αβγ − γ2 + β2δ>0, α2β + β3 − αγ + βδ > 0.
There are two especially interesting physical cases of these equations: 358 NAWAF M. BOU-RABEE, JERROLD E. MARSDEN, AND LOUIS A. ROMERO
1. When δ>0, γ = β = 0, the system is neutrally stable with or without the presence of the gyroscopic term. Adding usual dissipation (β>0) makes the neutrally stable zero solution asymptotically stable. Adding, however, damping in rotational variables can stabilize or destabilize the neutrally stable zero solution. 2. When δ<0, α>−4δ>0, β = γ = 0, the system is gyroscopically, and hence neutrally, stable. Adding usual damping makes the neutrally stable zero solution asymptotically unstable since the second inequality in (2.2) can never hold. This case corresponds to the classical dissipation-induced instability [1]. If β = 0 and β>0, the neutrally stable zero solution becomes asymptotically unstable. Adding damping in both variables, i.e., β>0 and γ>0, can stabilize or destabilize the zero solution depending on the ratio of β to γ. For the tippe top, we will show that dissipation in rotational variables (or complex damping) is essential to understanding inversion. In fact, the remarks above point out some limitations of usual damping: usual damping can only predict instability in the case of a gyroscopically stable system and stability in the case of a gravitationally stable system. Consider the modified Maxwell–Bloch equations as a possible model of the linearized behavior of the tippe top. In particular, suppose that the noninverted and inverted states of the tippe top correspond to the zero solution of (2.1). In the inviscid case, we observe a noninverted state which is gravitationally stable with or without gyroscopic effects. Remark 1 above shows that the addition of usual damping cannot destabilize this gravitationally stable, noninverted state. The complex damping term, however, can destabilize this state. Therefore, the complex damping term can explain why the gravitationally stable tippe top becomes asymptotically unstable. Moreover, after the tippe top inverts we have a gyroscopically stabilized inverted state. We have shown that the addition of usual damping would make such a system asymptotically unstable. Thus, usual damping cannot explain why the tippe top spins stably in its inverted state. Remark 2 shows that the complex and usual damping term in the right ratio can, however, stabilize this state. Thus, the complex damping term can also explain why the tippe top spins stably on its stem. We will revisit this analysis when we cast the linearized equations of the tippe top in the form of the modified Maxwell–Bloch equations. 3. Tippe top governing equations. This section contains a pedagogical derivation of the tippe top governing equations following Or [11], given mainly for the reader’s convenience. The section concludes with a brief discussion of how to explicitly obtain the equations derived by Or [11] and Ebenfeld and Scheck [6] from our form of the equations and how to formulate the equations of motion using Lagrangian mechanics. Derivation. We write the equations of motion of the tippe top from first principles. We idealize the tippe top as a ball of radius R and mass M on a fixed plane. The mass distribution of the ball is inhomogeneous, but symmetric about an axis through the ball’s geometric center. Thus, the ball’s center of mass is located on the axis of symmetry k, which is pointing in the direction (l, m, n), but at a distance Re above the geometric center, where e is the center of mass offset (0 ≤ e ≤ 1). Let the points Q, O, and C represent the point of contact, the geometric center, and the center of mass of the ball, respectively (cf. Figure 3.1). We define ex, ey, ez to be unit vectors TIPPE TOP INVERSION 359 of a nonrotating Cartesian frame attached to O. We define principal axes as i, j, k with axis of symmetry k. Let L, ω, (X, Y, Z) be the ball’s angular momentum about O, angular velocity, and absolute position of its center of mass, respectively. We define Ik and I = Ii = Ij to be the inertias about the respective principal axes attached to O. Let the vector Q represent the position of the point of contact Q with respect to the center of mass O given by